白云-荔湾凹陷珠江组大型深水水道体系沉积特征及成因机制

廖计华; 徐强; 陈莹; 王颖; 蔡露露; 邹梦君; 曾清波; 焦振华

doi:10.3799/dqkx.2016.086

Volume 41 Issue 6

Jun. 2016

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2016 > 41(6): 1041-1054

Liao Jihua, Xu Qiang, Chen Ying, Wang Ying, Cai Lulu, Zou Mengjun, Zeng Qingbo, Jiao Zhenhua, 2016. Sedimentary Characteristics and Genesis of the Deepwater Channel System in Zhujiang Formation of Baiyun-Liwan Sag. Earth Science, 41(6): 1041-1054. doi: 10.3799/dqkx.2016.086

Citation:

Liao Jihua, Xu Qiang, Chen Ying, Wang Ying, Cai Lulu, Zou Mengjun, Zeng Qingbo, Jiao Zhenhua, 2016. Sedimentary Characteristics and Genesis of the Deepwater Channel System in Zhujiang Formation of Baiyun-Liwan Sag. Earth Science, 41(6): 1041-1054. doi: 10.3799/dqkx.2016.086

Citation:

Liao Jihua, Xu Qiang, Chen Ying, Wang Ying, Cai Lulu, Zou Mengjun, Zeng Qingbo, Jiao Zhenhua, 2016. Sedimentary Characteristics and Genesis of the Deepwater Channel System in Zhujiang Formation of Baiyun-Liwan Sag. Earth Science, 41(6): 1041-1054. doi: 10.3799/dqkx.2016.086

PDF( 5481 KB)

Sedimentary Characteristics and Genesis of the Deepwater Channel System in Zhujiang Formation of Baiyun-Liwan Sag

doi: 10.3799/dqkx.2016.086

Research Institute of CNOOC, Beijing 100028, China

Received Date: 2015-12-10
Publish Date: 2016-06-15

Abstract

Abstract

The deepwater channel system is a large-scale deepwater sedimentary system which was newly found in abyssal mudstone of the upper Zhujiang Formation, eastern margin of Baiyun-Liwan sag in recent years. However, its sedimentary characteristics, sedimentary processes and main controlling factors are unclear yet.Based on substantial 2-D, 3-D seismic and well logging data, the depositional elements, geometry, internal architecture and sedimentary evolution of the deepwater channel system in Miocene Zhujiang Formation of Baiyun-Liwan sag were studied. In addition, the source supply, shelf break belt, palaeogeomorphology and their controlling effects on distribution, internal architecture and evolution of the deepwater channel system were discussed. Finally, the genetic mechanism of it was built.The results show that the deepwater channel system consists of channel, levee, and lobe, and channel is the primary depositional element. The deepwater channel can be subdivided into Baiyun sag segment, southern uplift segment and Liwan sag segment from north to south, which is mainly erosional channel, erosional-aggradational channel and aggradational channel, respectively. And it presents an evolutionary characteristic of "third-order channel" from north to south because the energy of gravity flow weakened by descending order. Two periods of channel evolution in vertical succession can be identified in each segment by identifying secondary erosional surfaces in the interior of channel. And there are distinctive internal filling properties in different channel evolution and different segments because of different fillings and transformation processes. The formation and development of deepwater channel system resulted from the interaction between the northern Pearl River Delta, shelf break belt and restricted paleotopography in eastern Baiyun-Liwan sag.
- deepwater channel system,
- Baiyun sag,
- Liwan sag,
- Zhujiang Formation,
- Pearl River Mouth Basin,
- deepwater exploration,
- petroleum geology

FullText(HTML)

References(39)

References

Abreu, V., Sullivan, M., Pirmez, C., et al., 2003.Lateral Accretion Packages (LAPs):An Important Reservoir Element in Deep-Water Sinuous Channels.Marine and Petroleum Geology, 20(6):631-648.doi: 10.1016/j.marpetgeo.2003.08.003

Gong, Z.S., Li, S.T., Xie, T.J., et al., 1997.Continental Margin Basin Analysis and Hydrocarbon Accumulation of the Northern South China Sea.Science Press, Beijing (in Chinese).

Jiang, S., Wang, H., Weimer, P., 2008.Sequence Stratigraphy Characteristics and Sedimentary Elements in Deepwarter.Earth Science, 33(6):825-833 (in Chinese with English abstract). http://earth-science.net/WebPage/Article.aspx?id=1774

Khain, V.E., Polyakova, I.D., 2004.Oil and Gas Potential of Deep-and Ultradeep-Water Zones of Continental Margins.Lithology and Mineral Resources, 39(6):530-540.doi: 10.1023/B:LIMI.0000046956.08736.e4

Kolla, V., Bourges, P., Urruty, J.M., et al., 2001.Evolution of Deep-Water Tertiary Sinuous Channels Offshore Angola (West Africa) and Implications for Reservoir Architecture.AAPG Bulletin, 85(8):1373-1405.doi: 10.1306/8626CAC3-173B-11D7-8645000102C1865D

Li, S.L., Yu, X.H., Liu, Y.M., et al., 2012.Formation Mechanism and Pattern of Deep-Water Fan with Channel and Lobe:A Case Study of Zhujiang Formation in Liwan3-1 Area, Baiyun Depression.Earth Science Frontiers, 19(2):33-40 (in Chinese with English abstract). http://www.sciencedirect.com/science/article/pii/S0264817216304548

Liu, B.J., Pang, X., Yan, C.Z., et al., 2011.Evolution of the Oligocene-Miocene Shelf Slope-Break Zone in the Baiyun Deep-Water Area of the Pearl River Mouth Basin and Its Significance in Oil-Gas Exploration.Acta Petrolei Sinica, 32(2):234-242 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYXB201102008.htm

Liu, S.Q., Zhang, C.M., Sun, Z., et al., 2016.Characteristics and Significances of the Geological Boundary SB21 in the Zhujiang Formation of the Liwan Sag, Pearl River Mouth Basin.Earth Science, 41(3):475-485 (in Chinese with English abstract). http://earth-science.net/WebPage/Article.aspx?id=3264

Liu, X.Y., Yu, S., Tao, W.X., et al., 2012.Filling Architecture and Evolution of Upper Miocene Deep-Water Channel in Congo Fan Basin.Earth Science, 37(1):105-112 (in Chinese with English abstract). http://earth-science.net/WebPage/Article.aspx?id=2204

Mayall, M., Jones, E., Casey, M., 2006.Turbidite Channel Reservoirs-Key Elements in Facies Prediction and Effective Development.Marine and Petroleum Geology, 23(8):821-841.doi: 10.1016/j.marpetgeo.2006.08.001

Moody, J.D., 2012.Quantitative Outcrop Characterization of an Analog to Weakly Confined Submarine Channel Systems:Morillo 1 member, Ainsa Basin, Spain.AAPG Bulletin, 96(10):1813-1841.doi: 10.1306/01061211072

Morgan, R., 2004.Structural Controls on the Positioning of Submarine Channels on the Lower Slopes of the Niger Delta.In:Davies, R.J., Cartwright, J., Stewart, S.A., et al., eds., 3D Seismic Technology:Application to the Exploration of Sedimentary Basins.Geological Society London Memoirs, 29(1):45-51.doi:10.1144/GSL.MEM.2004.029.01.05

Pang, X., Chen, C.M., Peng, D.J., et al., 2008.Basic Geology of Baiyun Deep-Water Area in the Northern South China Sea.China Offshore Oil and Gas (Geology), 20(4):215-222 (in Chinese with English abstract). https://www.researchgate.net/publication/284079507_Basic_geology_of_Baiyun_deepwater_area_in_the_northern_South_China_Sea

Pang, X., Shen, J., Yuan, L.Z., et al., 2006.Petroleum Prospect in Deepwater Fan System of the Pearl River in the South China Sea.Acta Petrolei Sinica, 27(3):13-21 (in Chinese with English abstract). https://www.researchgate.net/publication/292805775_Petroleum_prospect_in_deep-water_fan_system_of_the_Pearl_River_in_the_South_China_Sea

Wang, W., Ye, J.R., Yang, X.H., et al., 2015.Sediment Provenance and Depositional Response to Multistage Rifting, Paleogene, Huizhou Depression, Pearl River Mouth Basin.Earth Science, 40(6):1061-1071 (in Chinese with English abstract). http://earth-science.net/WebPage/Article.aspx?id=3103

Wu, J.F., Xu, Q., Zhu, Y.H., 2010.Generation and Evolution of the Shelf-Edge Delta in Oligocene and Miocene of Baiyun Sag in the South China Sea.Earth Science, 35(4):681-690 (in Chinese with English abstract). http://earth-science.net/WebPage/Article.aspx?id=2011

Wu, S.G., Qin, Y.S., 2009.The Research of Deepwater Depositional System in the Northern South China Sea.Acta Sedimentologica Sinica, 27(5):923-930 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201204003.htm

Wynn, R.B., 2007.Sinuous Deep-Water Channels:Genesis, Geometry and Architecture.Marine and Petroleum Geology, 24(6):341-387.doi: 10.1016/j.marpetgeo.2007.06.001

Xie, X.N., Chen, Z.H., Sun, Z.P., et al., 2012.Depositional Architecture Characteristics of Deepwater Deposition Systems on the Continental Margins of Northwestern South China Sea.Earth Science, 37(4):627-634 (in Chinese with English abstract). http://earth-science.net/WebPage/Article.aspx?id=2269

Yang, C.H., Du, X., Pan H.S., et al., 2000.Advances in Worldwide Deepwater Hydrocarbon Exploration and Oil and Gas Exploration Potential in the Northern Continental in the Northern Continental Slope in South China Sea.Earth Science Frontiers, 7(3):247-256 (in Chinese with English abstract). https://www.researchgate.net/publication/292434203_Advances_of_oil_and_gas_explorations_in_worldwide_deepwater

Zeng, Q.B., Wu, J.F., Zhao, Z.G., et al., 2013.Discovery and Exploratory Significance of a Deep-Water Channel System in Zhujiang Formation, Baiyun-Liwan Sag, Pearl River Mouth Basin.Acta Petrolei Sinica, 34(S2):1-9 (in Chinese with English abstract). https://www.researchgate.net/publication/273791493_Hydrocarbon_accumulation_conditions_and_exploration_direction_of_Baiyun-Liwan_deep_water_in_the_Pearl_River_Mouth_Basin

Zhang, G.C., Mi, L.J., Wu, S.G., et al., 2007.Deepwater Area?the New Prospecting Targets of Northern Continental Margin of South China Sea.Acta Petrolei Sinica, 28(2):16-20 (in Chinese with English abstract). https://www.researchgate.net/publication/279551230_Deepwater_area_-_The_new_prospecting_targets_of_northern_continental_margin_of_South_China_Sea

Zhu, W.L., Zhang, G.C., Gao, L., 2008.Geological Characteristics and Exploration Objectives of Hydrocarbons in the Northern Continental Margin Basin of South China Sea.Acta Petrolei Sinica, 29(1):1-9 (in Chinese with English abstract). doi: 10.1111/j.1745-7254.2008.00742.x

龚再升, 李思田, 谢泰俊, 等, 1997.南海北部大陆边缘盆地分布与油气聚集.北京:科学出版社.

蒋恕, 王华, Weimer, P., 2008.深水沉积层序特点及构成要素.地球科学, 33(6): 825-833. http://earth-science.net/WebPage/Article.aspx?id=1774

李胜利, 于兴河, 刘玉梅, 等, 2012.水道加朵体型深水扇形成机制与模式:以白云凹陷荔湾3-1地区珠江组为例.地学前缘, 19(2): 33-40. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201202007.htm

刘思青, 张翠梅, 孙珍, 等, 2016.珠江口盆地荔湾凹陷珠江组关键地质界面SB21的识别及地质意义.地球科学, 41(3): 475-485. http://earth-science.net/WebPage/Article.aspx?id=3264

刘新颖, 于水, 陶维祥, 等, 2012.刚果扇盆地上中新世深水水道充填结构及演化特征.地球科学, 37(1): 105-112. http://earth-science.net/WebPage/Article.aspx?id=2204

柳保军, 庞雄, 颜承志, 等, 2011.珠江口盆地白云深水区渐新世-中新世陆架坡折带演化及油气勘探意义.石油学报, 32(2): 234-242. doi: 10.7623/syxb201102007

庞雄, 陈长民, 彭大钧, 等, 2008.南海北部白云深水区之基础地质.中国海上油气(地质), 20(4): 215-222. http://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD200804002.htm

庞雄, 申俊, 袁立忠, 等, 2006.南海珠江深水扇系统及其油气勘探前景.石油学报, 27(3): 13-21. http://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200603002.htm

王维, 叶加仁, 杨香华, 等, 2015.珠江口盆地惠州凹陷古近纪多幕裂陷旋回的沉积物源响应.地球科学, 40(6): 1061-1071. http://earth-science.net/WebPage/Article.aspx?id=3103

吴景富, 徐强, 祝彦贺, 2010.南海白云凹陷深水区渐新世-中新世陆架边缘三角洲形成及演化.地球科学, 35(4): 681-690. http://earth-science.net/WebPage/Article.aspx?id=2011

吴时国, 秦蕴珊, 2009.南海北部陆坡深水沉积体系研究.沉积学报, 27(5): 923-930. http://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201303015.htm

解习农, 陈志宏, 孙志鹏, 等, 2012.南海西北陆缘深水沉积体系内部构成特征.地球科学, 37(4): 627-634. http://earth-science.net/WebPage/Article.aspx?id=2269

杨川恒, 杜栩, 潘和顺, 等, 2000.国外深水领域油气勘探新进展及我国南海北部陆坡深水区油气勘探潜力.地学前缘, 7(3): 247-256. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200003030.htm

曾清波, 吴景富, 赵志刚, 等, 2013.珠江口盆地白云-荔湾深水区珠江组大型水道体系的发现与勘探意义.石油学报, 34(S2): 1-9. doi: 10.7623/syxb2013S2001

张功成, 米立军, 吴时国, 等, 2007.深水区——南海北部大陆边缘盆地油气勘探新领域.石油学报, 28(2): 16-20. http://www.cnki.com.cn/Article/CJFDTOTAL-SYXB200702002.htm

朱伟林, 张功成, 高乐, 2008.南海北部大陆边缘盆地油气地质特征与勘探方向.石油学报, 29(1): 1-9. doi: 10.7623/syxb200801001

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(12)

Get Citation

PDF

XML

Article views (5205) PDF downloads(63)

Sedimentary Characteristics and Genesis of the Deepwater Channel System in Zhujiang Formation of Baiyun-Liwan Sag

doi: 10.3799/dqkx.2016.086

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content